气候变化领域集成服务门户(CCPortal): Carbonates before skeletons: A database approach

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DOI	10.1016/j.earscirev.2019.103065
	Carbonates before skeletons: A database approach
	Cantine M.D.; Knoll A.H.; Bergmann K.D.
发表日期	2020
ISSN	0012-8782
卷号	201
英文摘要	Carbonate minerals have precipitated from seawater for at least the last 3.8 billion years, but changes in the physical and chemical properties of carbonate rocks demonstrate that the nature, loci, and causes of this precipitation have varied markedly through time. Biomineralization is perhaps the most obvious time-bounded driver. However, other changes in the sedimentological character of Archean and Proterozoic carbonates offer an under-considered record of fluctuations in Earth's chemical, biological, and physical systems before and during the rise of animal life. Geobiologists and geochemists have successfully used large geochemical datasets to track changes in Earth's surface chemistry through time, but inconsistencies between proxies make the recognition of clear spatial-temporal patterns challenging. In order to place new constraints on the environmental history of Archean and Proterozoic oceans, especially with regard to redox state, we present for the first time a high-resolution database of global Precambrian and Cambrian carbonate sedimentation. Our initial datasbase, named Microstrat, comprises carbonate-bearing successions dating from c. 3.4 billion to ~500 million years old; these include more than 130 carbonate-bearing formations, digitized at the highest stratigraphic resolution possible and classified by environment of deposition. Lithofacies details are recorded at the finest scale available, including a range of microbial and other depositional fabrics, mineralogy, environment of deposition, age and location. We interrogate the Archean, Proterozoic, and Cambrian carbonate records, testing both long-standing and novel hypotheses about changes in Earth's carbonate system through time. Changes in carbonate sedimentology illuminate global changes in bioturbation and microbial community structure; the depth-dependent timing of marine oxygenation and the transition from anaerobic to aerobic respiration at and within the seafloor; and temporal changes in patterns of dolomitization. Shifts in both the loci of carbonate precipitation and in markers of animal activity are consistent with time- and depth-dependent trends in ocean oxygenation. We also note changes through time in the morphologies of stromatolites and thrombolites, which we suggest reflect secular shifts in carbonate precipitation, clastic sediment transport, and eukaryotic evolution. Observations from the database and petrographic studies confirm that the nature and extent of Proterozoic dolomite contrasts with that of dolomite in the Phanerozoic, consistent with dolomite being an early or even, in some cases, primary precipitate prior to the Cambrian Period. Because this database preserves environmental context and the stratigraphic relationships of carbonate features rather than tracking the occurrence of single features through time, it permits new and detailed analyses of the physical sedimentology of Precambrian carbonates and correlations in time and space among different features. We also consider how to build upon this initial dataset. Capturing and analyzing sedimentological data is difficult. Analysis becomes more challenging when data have been collected by multiple researchers working across Earth's entire history and surface. Field observations have a great deal of power to describe and explain changes in Earth's surface environments, yet they are often reported in idiosyncratic ways that make it difficult to compare them, obscuring their true explanatory power. Microstrat is an effort to pool idiosyncratic sedimentological data in hopes of illuminating Archaean, Proterozoic, and Cambrian carbonate depositional environments, yet it is unavoidably limited. We describe how other researchers can help to build Microstrat into a community-curated database by reporting and sharing data. © 2020 Elsevier B.V.
英文关键词	Carbonate facies; Carbonate precipitation; Dolomite; Intraclasts; Molar tooth structures; Ooids; Seafloor precipitate textures; Stromatolites
语种	英语
scopus关键词	Archean; Cambrian; carbonate group; carbonate sediment; dolomite; facies; ooid; precipitation (chemistry); Proterozoic; seafloor; skeleton; stromatolite; tooth; Animalia; Eukaryota
来源期刊	EARTH-SCIENCE REVIEWS
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/209711
作者单位	Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, United States; Department of Organismic and Evolutionary Biology, Harvard University, Cambridge, MA 02138, United States
推荐引用方式 GB/T 7714	Cantine M.D.,Knoll A.H.,Bergmann K.D.. Carbonates before skeletons: A database approach[J],2020,201.
APA	Cantine M.D.,Knoll A.H.,&Bergmann K.D..(2020).Carbonates before skeletons: A database approach.EARTH-SCIENCE REVIEWS,201.
MLA	Cantine M.D.,et al."Carbonates before skeletons: A database approach".EARTH-SCIENCE REVIEWS 201(2020).